夏季索马里越赤道气流垂直结构的年代际变化  

The interdecadal variations of the vertical structure of the summer Somali cross-equatorial flow

作　　者：邱金晶 孙照渤[2] 邓伟涛[2] 

机构地区：[1]浙江省气象科学研究所,杭州310008 [2]南京信息工程大学气象灾害省部共建教育部重点实验室 大气科学学院,南京210044

出　　处：《气象学报》2014年第2期318-336,共19页Acta Meteorologica Sinica

基　　金：国家自然科学基金资助项目(40775059);国家自然科学基金青年科学基金项目(41205035);气象灾害省部共建教育部重点实验室开发课题(KLME1104);江苏省高校自然科学研究面上项目(10KJB170007);江苏高校优势学科建设工程资助项目(PAPD)

摘　　要：基于1950—2010年美国国家环境预报中心/国家大气研究中心(NCEP/NCAR)再分析月平均资料、哈得来中心月平均海温资料,定义夏季索马里越赤道气流(简称SMJ)垂直结构指数VS_1和VS_2,分别表征索马里越赤道气流全区一致、上下反相两种分布型。接着利用合成分析、奇异值分解方法探讨夏季索马里越赤道气流垂直结构的年代际变化,寻找可能影响其变化的环流因子和海温信号,并进一步分析垂直结构与亚洲夏季风活动的年代际关系,主要结论如下:(1)两个指数在年代际尺度上的阶段性变化特征十分显著,VS_1在20世纪80年代中期发生由负转正的年代际变化;VS_2在70年代初和90年代中期分别发生由负转正、由正转负的年代际变化。(2)合成分析表明,VS_1和VS_2的年代际变化与同期大气环流联系紧密,南极涛动可能是影响VS_1年代际变化的一个重要因子。(3)印度洋海温变化可能对夏季索马里越赤道气流两类垂直结构的年代际变化起调控指示作用。VS_1的年代际变化与夏季全印度洋海温增暖的趋势是一致的,VS_2与夏季南印度洋偶极型振荡事件关系显著。(4)高VS_1年代里,印度半岛至中南半岛夏季风偏弱,纬向水汽供应减少,降水偏少,东亚夏季风亦偏弱,使得华北地区纬向和经向水汽输送均偏弱,同时水汽辐合减弱,华北地区偏旱,而在江南地区由于水汽辐合,降水偏多;反之亦然。高VS_2年代,东亚季风区内中国西南、华南地区夏季风减弱,使得经向和纬向水汽输送均偏弱,水汽供应减少,因此华南、西南地区偏旱,日本地区夏季风偏弱,西风水汽输送亦偏弱,降水亦偏少,反之亦然。Based on the 1950-2010 NECP/NCAR reanalysis monthly mean data and the Hadley monthly mean SST,the two indices,denoted by VS1 and VS2 ,are defined,which are able to describe the variabilities of the two vertical modes,called the consistent mode and the vertically opposite mode,of the summertime Somali cross-equatorial flow （SMJ）.Using the singular value decomposition （SVD）and the composite analysis,it is mainly done in this paper to analyse the interdecadal variations of the vertical structures of SMJ and the associated atmospheric circulation features,as well as the SST signals.The relationships between the indices and Asia summer monsoon activity are also discussed.The results show that：（1）VS1 and VS2 exhibit ob-vious interdecadal variabilities.In the study time of interest,the former turns positive in the mid-1980s,the later experiences two decadal mutations,one is from positive to negative in the early 1970s and the other is from negative to positive in the late 1990s.（2）The composite analysis indicates that the interdecadal variabilities of VS1 and VS2 are closely related to the atmos-phere circulation.It＇s also worth mentioning that the Antarctic Oscillation （AAO）may be an important factor which effects the interdecadal changes of VS1 .（3）The SSTA in the Indian Ocean could play the regulating and indication role in the interdecadal variations of the vertical structures of SMJ.VS1 is found to be in line with the trend seen in SSTA of the whole Indian Ocean. VS2 is related to the Southern Indian Ocean SST anomaly dipole oscillation.And,（4）on interdecadal timescale,when VS1 is in a positive phase,the summer monsoon weakens,and accordingly,the zonal moisture supply over the Indian peninsula to the Indo-China Peninsula reduces with the summer rainfall tending to be less than normal.At the same time,the relatively weak East Asia summer monsoon,the related weak moisture transportation and the weak moisture convergence lead to more rainfall in North China.More rainfall occurs in the s

关 键 词：索马里越赤道气流垂直结构 年代际变化 大气环流 海温 夏季风活动 

分 类 号：P434[天文地球—大气科学及气象学] P461